Edexcel B GCSE Geography > Hazardous Earth > What are volcanic hotspots?
Volcanoes are most common at plate boundaries, but some form in the middle of tectonic plates, far away from any boundary. Hotspots create these unusual volcanoes.
What is a hotspot?
A volcanic hotspot is an area where a column of very hot mantle rock, called a mantle plume, rises towards the Earth’s surface.
This heat melts the base of the lithosphere, causing magma to break through the crust and form volcanoes.
Hotspots can occur:
beneath oceanic crust (e.g. Hawaii)
beneath continental crust (e.g. Yellowstone, USA)
How do hotspots form volcanoes?
Hot mantle rock rises in a narrow plume.
The heat melts the crust above it.
Magma reaches the surface and forms a volcano.
As the tectonic plate slowly moves, the hotspot stays in the same place.
New volcanoes form above the plume, while older ones move away and become extinct.
This creates a chain of volcanoes, lined up in the direction the plate is moving.
Key features of hotspot volcanoes
They produce runny, basaltic lava, similar to volcanoes at divergent boundaries.
Eruptions tend to be frequent but less explosive.
Over time, repeated eruptions can build shield volcanoes. wide volcanoes with gentle sides.